Page 102 - Formation Damage during Improved Oil Recovery Fundamentals and Applications
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84                                                  Thomas Russell et al.


             Which of the two minima should be used is still a matter of some
          contention. Some authors suggest that the electrostatic force experienced
          when leaving the primary minimum is too great for any other forces to
          detach the particle; hence, all particles that can detach must have resided
          in the secondary minimum. On the other hand, as outlined in the low-
          salinity curve in Fig. 3.6, some potential energy profiles either do not
          have secondary minima, or they are too small to prevent particles from
          freely leaving due to Brownian motion (Bradford et al., 2013).
             Calculations for gravitational and lift forces indicate that their order of
          magnitude range is between 10 214  and 10 213 , although drag and electro-
                                     211       28
          static forces range between 10  and 10  (Bedrikovetsky et al., 2012;
          Kalantariasl and Bedrikovetsky, 2013). Therefore, gravitational and lift
          forces are disregarded and only drag and electrostatic forces are considered
          to be relevant to determine conditions for particle detachment.
          Calculations of the torque balance will only take into account drag and
          electrostatic forces and thus, Eq. (3.1) simplifies to the following form:

                                                   ð
                            F d U; r s Þ 5 F e r s ; γ; pH; Tð  Þlr s ; F e Þ;  (3.15)
                              ð
             Favorable conditions for particle mobilization happen when the drag
          torque exceeds the electrostatic torque. If the particle is attached to the
          pore surface, this means that it is in a stable equilibrium, where the net
          force on the particle is zero.
             The equations for lever arms, drag, and electrostatic forces provide an
          understanding of which parameters can lead to favorable conditions for
          particle detachment during waterflooding. The drag force is mainly a
          function of velocity and particle size. The higher the carrier fluid velocity
          and particle size, the higher the drag force, increasing the likelihood of
          particle detachment. The electrostatic force is primarily affected by water
          salinity, pH, and temperature. The attractive London-Van der Waals
          potential and repulsive Born potential are functions of the Hamaker
          constant, which is a function of the dielectric constant and refractive
          index for particle, grain, and fluid, both are temperature dependent
          (Israelachvili, 2011). An increase in the temperature will increase repul-
          sion between the particle and surface. The repulsive electrical double
          layer is a function of the inverse Debye length and zeta potentials. The
          first is inversely proportional to the water salinity and pH, meaning that
          lower salinity and higher pH will lead to higher repulsion between parti-
          cle and surface. The second is a function of pH and temperature, higher
          pH and temperature will also lead to stronger repulsion. Thus, high pH
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